Abstract

Conceptual rainfall-runoff models besides precipitation and discharge data generally require estimates of the mean daily air temperature as input data. For the estimation of the mean daily air temperature, there are different methods available. The paper presents an evaluation of the impact of the mean daily air temperature calculation on the rainfall-runoff modelling results. Additionally, other measured variables and rating curve uncertainty were assessed. Differences in the mean daily air temperature values were evaluated for the 33 meteorological stations in Slovenia and additional investigations were conducted for four selected meso-scale catchments located in different climates. The results of the application of four equations for the mean air temperature calculation yielded the mean absolute error values between 0.56–0.80 °C. However, the results of rainfall-runoff modelling showed that these differences had an almost negligible impact on the model results. Differences in the mean simulated discharge values were no larger than 1%, while differences in the maximum discharge values were a bit larger, but did not exceed 5%. A somewhat larger impact on the model results was observed when precipitation and water level measurements’ uncertainty was included. However, among all analysed input data uncertainties, the rating curve uncertainty can be regarded as the most influential with differences in the simulated mean discharge values in the range of 3% and differences in the maximum discharge values up to 14%.

Highlights

  • In recent decades, numerous rainfall-runoff models have been developed [1,2]

  • One can notice that Equations (2) and (3) yielded relatively similar Mean Absolute Error (MAE) values (Figure 2)

  • Equation (3) as well as Equation (2), which is very frequently used in Slovenia for the Equation (3) as well as Equation (2), which is very frequently used in Slovenia for the calculation of the mean daily air temperature, both yield similar MAE values in case Equation (1)

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Summary

Introduction

Numerous rainfall-runoff models have been developed [1,2]. These types of models can be used for various applications such as water management, engineering design, climate change studies, risk management, etc. Precipitation and discharge data are the main input variables in all types of rainfall-runoff models. Some model types such as conceptual (i.e., storage-based) rainfall-runoff models require other input data such as potential evapotranspiration [2]. Models with an included snow module require air temperature data to account for snow accumulation and melting processes since temperature is the main driver of snow-rain partition [2,4,9,10].

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